Sydney sits on the Triassic Sydney Basin, a sequence of Hawkesbury Sandstone, Ashfield Shale, and Quaternary alluvium. The city's population exceeds 5.3 million, and many suburbs lie on deep soil profiles over bedrock. MASW surveys measure shear wave velocity (VS) from surface waves to map stiffness contrasts. This is critical for seismic design under AS/NZS 1170.4. The VS30 parameter — the average shear wave velocity in the top 30 metres — classifies sites from Class A (hard rock) to Class E (soft soil). Without it, designers cannot determine the correct spectral shape for earthquake loads. Combining MASW with a dilatometer test provides complementary stiffness data at depth, while microtremor HVSR confirms resonance frequencies independently.

MASW provides a continuous VS profile from a single surface line — no boreholes needed. It is the fastest method for site class assignment in the Sydney Basin.